四川木里梭罗沟金矿床特征  

Geological Features of the Suoluogou Au Deposit in Muli, Sichuan

作　　者：喻安光[1] 卢玫瑰[1] 宋晓华[1] 刘文武[1] 

机构地区：[1]四川省地质矿产勘查开发局区域地质调查队,成都610213

出　　处：《四川地质学报》2014年第4期514-516,共3页Acta Geologica Sichuan

摘　　要：四川木里梭罗沟金矿床位于甘孜—理塘构造成矿带的南段、唐央复式背斜南东倾伏端(或唐央穹窿南缘),目前已探明储量属大型岩金矿床。矿体产于上三叠统曲嘎寺组蚀变基性火山岩中,受近东西向断裂控制。矿床具多期成矿特点,属构造蚀变岩型—中低温热液型金矿床。The Suoluogou Au deposit in Muli, Sichuan lies on the southern margin of the Tangyang dome in the southern section of the Garze-Litang tectonic-metallogenic belt. The deposit is confined to the altered basic volcanic rock of the Upper Triassic Qugasi Formation and controlled by nearly EW-trending fracture zone The deposit is a structural altered rock type one which was formed by multiple ore-formation.

关 键 词：金矿床 控矿断裂 多期成矿 梭罗沟 

分 类 号：P618.4[天文地球—矿床学]